在受到厄尔尼诺/南方振荡影响的亚马逊洪水平原上偶尔堆积沉积物
Rolf Aalto1, Laurence Maurice-Bourgoin, Thomas Dunne
1Quaternary Research Center University of Washington, Seattle, Washington 98195, USA. aalto@geomorphology.com
Nature
|October 3, 2003
概括
由拉尼娜事件驱动的偶发性洪水,每8年左右在安第斯-亚马逊河流泛滥平原中沉积大量沉积物. 这些事件控制了洪水平原的形成和沉积物向亚马逊河的输送.
科学领域:
- 地球科学 地球科学 地球科学
- 水文学 水文学
- 沉积物学的沉积物学
背景情况:
- 大陆河流带有沙床在洪水平原中储存大量沉积物.
- 之前的研究确定了洪水平原在十年级的积累,但缺乏事件分辨率.
研究的目的:
- 调查安第斯山脉和亚马逊山脉林地中的沉积物积累模式.
- 识别离散的沉积物沉积事件和近一年的时间表.
主要方法:
- 从沉积物核中分析210Pb活动概况.
- 在亚马逊流域内,贝尼和马莫雷河流域 (720,000平方公里) 的研究地点.
主要成果:
- 沉积物层学主要由离散的,年龄均的沉积物包 (20-80厘米厚) 主导.
- 这些沉积事件的全系统复发间隔大约为8年.
- 插曲性事件与与拉尼尼亚事件相关的极端洪水有关.
结论:
- 由厄尔尼诺/南方振荡周期驱动的过渡过程控制了玻利维亚洪水平原的形成.
- 这些事件调节了下游沉积物,碳,营养和污染物向亚马逊河的输送.
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